wind stress वाक्य
उदाहरण वाक्य
मोबाइल
- A consequence of the Ekman theory explains that oceanic flow at the surface is directed at 45 degrees to the right of the wind stress in the Northern Hemisphere.
- Surface oceanic currents are sometimes wind driven and develop their typical clockwise spirals in the northern hemisphere and counter-clockwise rotation in the southern hemisphere due to imposed wind stresses.
- Physically, this implies that the altered convection in the Pacific Ocean due to El Ni�o drives changes in the meridional gradient of wind stress curl over the equatorial Atlantic.
- The structure of a subtropical frontal zone results in the formation of a positive wind stress curl, which is the shear stress exerted by wind on the surface of water.
- For example, positive ( eastward ) anomalies in wind stress in the central Pacific excite positive anomalies in 20�C isotherm depth which propagate to the east as equatorial Kelvin waves.
- This is strikingly similar to the wind stress anomalies seen in the Pacific during El Ni�o ( or La Ni�a ) events, although centered farther west in the Atlantic basin.
- Wind stresses cause a phenomenon referred to as " wind set-up ", which is the tendency for water levels to increase at the downwind shore, and to decrease at the upwind shore.
- Sverdrup theory succinctly summarizes this phenomenon mathematically by defining a geostrophic mass transport per unit latitude, M, as the east-west integral of the meridional derivative of wind stress curl, minus any Ekman transport.
- A warm anomaly is associated with relaxed trade winds across a large swath of the equatorial Atlantic basin, while a cool anomaly is associated with enhanced easterly wind stress in the same region.
- In this simple, modeling setting, the principal factors that were accounted for influencing the oceanic circulation were surface wind stress, bottom friction, a variable surface height leading to horizontal pressure gradients, and finally, the Coriolis effect.
- By assigning varying values for wind stress and surface heat flux, they were able to develop parameterizations for mixing depth and turbulent diffusivity using the LES model, and apply them to a phytoplankton model to monitor the response.
- A strong seasonality is also observed with respect to the remote, North Pacific influence in the tropical Atlantic, via ENSO events that induce western equatorial wind stress anomalies ( WEA ), which in return modulate the tropical Atlantic ocean-atmosphere dynamics.
- When the isle's red cedars proved too gnarled and knotty from salt and wind stress to be turned into pencil slats, he had the vision to secure it as a family retreat and, as much as possible, leave it be.
- Where h is the upper-layer thickness anomaly, ? is the wind stress, c is the Rossby wave speed that depends on latitude, ? 0 is the density of sea water and f 0 is the Coriolis parameter at a reference latitude.
- During anticyclonic regimes where the wind stress curl is negative freshwater is pumped into the Beaufort Gyre; during cyclonic regimes where wind stress curl is positive freshwater is released into the Arctic Ocean, where it can then flow into the North Atlantic.
- During anticyclonic regimes where the wind stress curl is negative freshwater is pumped into the Beaufort Gyre; during cyclonic regimes where wind stress curl is positive freshwater is released into the Arctic Ocean, where it can then flow into the North Atlantic.
- The maximum in freshwater content released into the ocean waters coincides with a maximum in wind stress curl ( i . e ., a minimum in Ekman pumping ), allowing for a high volume of freshwater to seep into the Arctic Ocean circulation.
- This form of wind stress causes hanging traffic lights to blow a foot or more up and down in the air, occasionally cartwheeling over and over, and, rarely, to crash down onto the streets below, becoming lethal at worst and useless at best.
- During April and May when the SST front is still strong, the seasonal warming makes the region conductive to atmospheric convection, and surface wind stress curls turn weakly positive along the front on the background of negative curls that drive the subtropical gyre.
- The result is that the models have very different wind stresses over the Southern Ocean, with the CM2.0 exhibiting the common bias of winds that are shifted equatorward but the CM2.1 model being one of the few that have winds close to the correct latitude and magnitude in this region ( Russell et al ., 2006 ).
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